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Record W2341160312

Abstract: How wet was it? A 5000 year wetland sediment record of changing moisture regimes in Nova Scotia

2011· article· en· W2341160312 on OpenAlexaffabout
Hilary White, Ian Spooner

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsAcadia University
Fundersnot available
KeywordsOutwash plainGeologyGlacial periodHoloceneWetlandPeatPalynologyRadiocarbon datingHydrology (agriculture)WoodlandWater tablePhysical geographyPaleontologyArchaeologyGroundwaterGeographyPollen
DOInot available

Abstract

fetched live from OpenAlex

Nova Scotia has one of the densest archives in Canada of regional paleoenvironmental data owing to the excellent preservation of Late Glacial and Early Holocene climate change records in lake sediments. Wetlands have received far less attention, though recent studies indicate that they have the potential to preserve long (9000+yr) and continuous records of past hydrogeological and moisture regimes. At the Pleasant River Fen (southwestern Nova Scotia) and Baltzer Bog (Annapolis Valley, Nova Scotia) excavated sections, gravity cores, and vibracores were used to expose sediment for stratigraphic analyses. Ages were obtained by conventional and AMS radiocarbon dating of terrestrial wood. Core samples were analyzed for lithostratigraphic proxies including loss on ignition (LOI) and magnetic susceptibility (MS). At Pleasant River Fen a transition in lithostratigraphic (MS and LOI) properties at 126 cm depth (~3000 14C yr BP) is a result of a rising water table and is coincident with a regime shift to moister and slightly cooler conditions as recorded in regional palynological records. Baltzer Bog is located in an elevated, closed basin located on an extensive glacial outwash deposit. Excavation and trenching exposed a ~2 m high continuous section of alternating wood and sphagnum dominated sediment. The base of the section is composed of glacial outwash sand that is directly overlain by coarse woody material which, in turn is overlain by a wetland assemblage. A conventional 14C date obtained on an upright stump at the initial woodland-wetland contact indicates an increase in local water table occurred shortly after 3070 ± 50 yr BP. Another woodland wetland transition was dated at 1730 ± 40 yr BP. A minimum of 4 transitions are evident, demonstrating that the water table at the site fluctuated substantially during the Late Holocene. Historical records show that over the past 200+ years the site has been in transition from wetland to woodland, an indication of a declining water table. Taken together these data indicate that rapid and substantial regional fluctuations in water table elevation occurred during the late Holocene. The rapid environmental change accompanying these fluctuations may have had a significant impact on several rare, disjunct species particular to wetlands, most notably the Blanding’s Turtle, the survival of which may be dependent on the stability of these environments.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.278
Threshold uncertainty score0.559

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.037
GPT teacher head0.242
Teacher spread0.205 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2011
Admission routes2
Has abstractyes

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